Scanning electron micrograph of dolomite. Dolomite is a carbonate mineral with a striking rhombohedric structure, revealed in stunning detail in this image. Dolomite is usually formed deep within the Eartha's crust, and geological deposits are now quite rare, however, it can also be formed naturally with the help of a sulphate-reducing bacterium. | |
Licence : | Droits gérés |
Crédit: | Science Photo Library / Science Source / Nano Creative |
Taille de l’image : | 5906 px × 4125 px |
Model Release : | Non requis |
Property Release : | Non requis |
Restrictions : | - |